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71.
Vertical migration of elements from mineral deposits 总被引:1,自引:0,他引:1
There is currently widespread interest in the exploration community worldwide in the development of methods to locate deeply buried mineralisation. In the application of geochemical methods, some success has been achieved using the selective extraction of mobile and weakly bonded forms of elements (MWBE) in overburden. Studies in Russia commenced in the 1960s, and have continued in Russia and in other countries to the present time. This paper presents some examples of experimental and applied research carried out in Russia, specifically by members of VITR and then VIRG NPO Rudgeofizika (St. Petersburg). In particular, some characteristics of MWBE anomalies and rates of MWBE migration are illustrated, with reference to several case studies in geochemical exploration for base metal and precious metal deposits. 相似文献
72.
Krzysztof Goździewski 《Celestial Mechanics and Dynamical Astronomy》1998,70(1):41-58
In this paper we consider the problem of motion of an infinitesimal point mass in the gravity field of an uniformly rotating
dumb-bell. The aim of our study is to investigate Liapunov stability of Lagrangian libration points of this problem. We analyze
the stability of libration points in the whole range of parameters ω, μ of the problem. In particular, we consider all resonance
cases when the order of resonance is not greater than five.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献
73.
川西螺髻山冰川侵蚀地貌研究 总被引:2,自引:4,他引:2
定量分析发现影响该地区冰斗形态的因素有海洋性较强的气候,朝向北(极向),朝向东和较大的地形起伏四种。槽谷的横剖面可以公式化为Y=a·X~b,槽谷形态不对称由冰川差异侵蚀和冻融差异所致。发现两种冰川侵蚀裂痕,即挤压剪切裂痕和拉张剪切裂痕。 相似文献
74.
为了快速查明古宁浑迪地区砂岩型铀矿的有利成矿地段,并为钻探验证工程的部署提供依据,研究过程中采用了铀及伴生元素活动态分量探测地球化学勘查方法。通过系统采集样品和铀、钼、硒分量提取及测试,认为吸附态铀及伴生元素分量探测更适用于本地区砂岩型铀成矿有利地段的筛选。经钻探工程验证,绝大部分地表铀分量异常均与深部成矿目的层中的铀矿化或铀异常相对应,证实了铀及伴生元素活动态分量探测是适用于寻找隐伏砂岩型铀矿床的有效方法,尤其适用于古河道型砂岩铀矿的找矿勘查。 相似文献
75.
76.
BAIOUM.H.M. 《中国地球化学学报》2002,21(3):215-226
The Campanian-Maastrichtian phosphatic deposits in Egypt,called the Duwi Forma-tion,comprise a part of the extensive Middle East to North African phosphogenic province of Late Cretaceous to Paleogene age.The province holds the greatest accumulation of phosphorites in the geological history,possibly in excess of 70 billion metric tons.The phosphate resources in Egypt alone exceed 3 billion metric tons.Two-third of these three billions occur only in the Abu-Tartur area.Among the phosphorite deposits in Egypt,the phosphorites of the Abu-Tartur area are characterized by high contents of iron ranging from 3% to 7% with an average of 5%.The detailed mineralogical and geochemical studies on the Abu-Tartur phosphorites revealed that iron is found in the form of pyrite,ankerite,clay minerals,microinclusions,and iron oxide.Pyrite,which is the major fraction,occurs as filling cement and partial to complete teplacement of phosphatic grains and confined to the fresh phosphorites while iron oxide occurs as cryp-tocrystalline aggregates of red to brown particles and is confined to the weathered outcrops.Ex-clusive relations between pyrite in the fresh phosphorite samples inside the Abu-Tartur mine and iron oxide in the equivalent horizon of the weathered exposure indicated that iron oxide was formed by the oxidation of pyrite as a result of weathering.All of these forms harm the quality of ore,manufacturing processes,and the produced phosphoric acid and fertilizers. 相似文献
77.
针对常规物化探方法对寻找砂岩型铀矿几乎无效这一现实,初步探讨了土壤元素有机结合态形成机理,并应用土壤有机结合态铀、钼测量法在新疆伊犁盆地南缘扎基斯坦地区进行了寻找地浸砂岩型铀矿试验。与全铀及210Po法测量结果对比表明,土壤有机结合态铀、钼异常能较好地反映埋深200 m以内的铀矿化,而全铀及210Po测量结果对深部砂岩型铀矿化几乎无任何显示。因此,土壤有机结合态铀、钼测量法有望成为地浸砂岩型铀矿找矿的有效方法。 相似文献
78.
Iréne Malmsten & Kurt Boström 《Geografiska Annaler: Series A, Physical Geography》2002,84(3-4):245-259
The Kärkejokk (jokk = Lappish for brook) is rich in sulfate and calcium, both elements having been considered enigmatic. To resolve these problems we collected waters at 13 sites during 27 June to 1 September 1996. Nine sites were in the Kärkevagge, and the others in the drainage towards lake Torne Träsk. Rain waters were collected the same period. Conductivity, pH, and temperature were measured in the field, whereas salt load and the elements Na, K, Ca, Mg, S, Si, Fe, Al, Mn, Zn, Sr, and Ba were determined in the laboratory.
Mixing models based on rain water and leaching products of the major bedrocks do not explain observed element patterns except in the lower parts of the jokk. However, oxidation of pyrite has formed acid, sulfate–rich solutions that released Ca and Mg from limestones, and Fe, Mn, Al, and Si, from black shales (Malmsten 1998; Malmsten et al. 2000). Conservative mixing models, using rain water, leached bedrock and pyrite, match the jokk waters quite well, and sulfur isotope data corroborate these findings. The nearby Låktajokk, and Vassijokk also contain much S.
Where these waters debouch they may deposit Si, Al, and Ca, but only little S on various rocks. Total rock analyses, thermodynamic and X–ray data suggest that gypsum, barite, or alunite are not formed in major quantities.
These models show that the hydrogeochemistry of the Kärkejokk may be less enigmatic than often assumed. 相似文献
Mixing models based on rain water and leaching products of the major bedrocks do not explain observed element patterns except in the lower parts of the jokk. However, oxidation of pyrite has formed acid, sulfate–rich solutions that released Ca and Mg from limestones, and Fe, Mn, Al, and Si, from black shales (Malmsten 1998; Malmsten et al. 2000). Conservative mixing models, using rain water, leached bedrock and pyrite, match the jokk waters quite well, and sulfur isotope data corroborate these findings. The nearby Låktajokk, and Vassijokk also contain much S.
Where these waters debouch they may deposit Si, Al, and Ca, but only little S on various rocks. Total rock analyses, thermodynamic and X–ray data suggest that gypsum, barite, or alunite are not formed in major quantities.
These models show that the hydrogeochemistry of the Kärkejokk may be less enigmatic than often assumed. 相似文献
79.
Armando Bazzani Stefano Marmi Giorgio Turchetti 《Celestial Mechanics and Dynamical Astronomy》1989,47(4):333-359
We prove that non resonant isochronous symplectic maps in a neighborhood of an elliptic fixed point are stable for exponentially long times with the inverse of the distance from the fixed point. In the proof we make use of the majorant series method together with an idea for optimizing remainder estimates first applied to Hamiltonian problems by Nekhoroshev. 相似文献
80.
钚是某些放射性废物中的关键核素,在放射性废物地质处置的过程中,钚的迁移行为研究对于处置库的安全评价至关重要。钚的存在形态直接影响其迁移行为,本文选用地球化学模式程序EQ3/6模拟计算了钚在某区钻孔地下水中的存在形态,并对影响因素进行了分析。结果表明某区地下水主要为咸水,具有高矿化的特征,pH值在7~9之间,水化学类型主要以Cl-SO4-Na型和SO4-Cl-Na型为主,地下水中钚的存在形态主要以Pu(Ⅳ)物种为主。并通过结论得出钚的存在形态主要受着地下水化学成分特征控制,同时pH值和Eh的值对钚的存在形态也有很大的影响。 相似文献